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From Greenhouse to Icehouse: Understanding Earth's Climate Extremes Through Models and Proxies.
by
Tabor
,
Clay
Richard
Published 2015
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Astronomy
Atmospheric
Earth system model simulations show a larger ice-volume response to obliquity than precession
Earth system model simulations show that the Late Cretaceous cooling was due to a reduction in CO2
Geology and Earth Sciences
Model results show that removal of regolith from the high-latitudes can explain the change in the ice-volume cycles across the Pleistocene
Oceanic and Space Sciences
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in agreement with ice-volume proxy records
not changes in paleogeography
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